Earth Science - Atmospheric Moisture

Earth Science - Atmospheric Moisture

Spahn's Science Lectures via YouTube Direct link

The temperature at which a dry parcel of air reaches saturation is known as the

17 of 17

17 of 17

The temperature at which a dry parcel of air reaches saturation is known as the

Class Central Classrooms beta

YouTube videos curated by Class Central.

Classroom Contents

Earth Science - Atmospheric Moisture

Automatically move to the next video in the Classroom when playback concludes

  1. 1 Intro
  2. 2 WATER'S CHANGES OF STATE: SOLID
  3. 3 LATENT HEAT
  4. 4 PHASE CHANGE DIAGRAM OF WATER
  5. 5 EVAPORATION AND CONDENSATION
  6. 6 SUBLIMATION AND DEPOSITION
  7. 7 HUMIDITY AND SATURATION
  8. 8 THE MIXING RATIO
  9. 9 RELATIVE HUMIDITY AND MOISTURE
  10. 10 RELATIVE HUMIDITY AND TEMPERATURE
  11. 11 DEW POINT TEMPERATURE
  12. 12 HOW IS HUMIDITY MEASURED?
  13. 13 More molecules are returning to the liquid state than are leaving the liquid state. This process is called
  14. 14 As a solid undergoes a phase change to a liquid, it
  15. 15 Which of the following processes absorbs or releases the most heat?
  16. 16 At 25°C it takes 20 grams of water vapor to saturate 1 kilogram of dry air. If there are 5 grams of water vapor in 1 km of air at that temperature, what is the relative humidity?
  17. 17 The temperature at which a dry parcel of air reaches saturation is known as the

Never Stop Learning.

Get personalized course recommendations, track subjects and courses with reminders, and more.

Someone learning on their laptop while sitting on the floor.